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通过综合方法确定的镁铝黑云母新活性模型。

A new activity model for Mg-Al biotites determined through an integrated approach.

作者信息

Dachs Edgar, Benisek Artur

机构信息

Fachbereich Chemie und Physik der Materialien, Abteilung Mineralogie, Universität Salzburg, Jakob-Haringerstrasse 2a, 5020 Salzburg, Austria.

出版信息

Contrib Mineral Petrol. 2019;174(9):76. doi: 10.1007/s00410-019-1606-2. Epub 2019 Aug 23.

Abstract

A new activity model for Mg-Al biotites was formulated through an integrated approach combining various experimental results (calorimetry, line-broadening in infrared (IR) spectra, analysis of existing phase-equilibrium data) with density functional theory (DFT) calculations. The resulting model has a sound physical-experimental basis. It considers the three end-members phlogopite (Phl, KMg[(OH)AlSiO]), ordered eastonite (Eas, KMgAl[(OH)AlSiO]), and disordered eastonite (dEas) and, thus, includes Mg-Al order-disorder. The DFT-derived disordering enthalpy, Δ , associated with the disordering of Mg and Al on the M sites of Eas amounts to 34.5 ± 3 kJ/mol. Various biotite compositions along the Phl-Eas join were synthesised hydrothermally at 700 °C and 4 kbar. The most Al-rich biotite synthesized had the composition = 0.77. The samples were characterised by X-ray diffraction (XRD), microprobe analysis and IR spectroscopy. The samples were studied further using relaxation calorimetry to measure their heat capacities ( ) at temperatures from 2 to 300 K and by differential scanning calorimetry between 282 and 760 K. The calorimetric (vibrational) entropy of Phl at 298.15 K, determined from the low- measurements on a pure synthetic sample, is = 319.4 ± 2.2 J/(mol K). The standard entropy, , for Phl is 330.9 ± 2.2 J/(mol K), which is obtained by adding a configurational entropy term, , of 11.53 J/(mol K) due to tetrahedral Al-Si disorder. This value is ~1% larger than those in different data bases, which rely on older calorimetrical data measured on a natural near-Phl mica. Re-analysing phase-equilibrium data on Phl + quartz (Qz) stability with this new , gives a standard enthalpy of formation of Phl, = - 6209.83 ± 1.10 kJ/mol, which is 7-8 kJ/mol less negative than published values. The superambient of Phl is given by the polynomial [J/(mol K)] as follows: . Calorimetric entropies at 298.15 K vary linearly with composition along the Phl-Eas join, indicating ideal vibrational entropies of mixing in this binary. The linear extrapolation of these results to Eas composition gives = 294.5 ± 3.0 J/(mol K) for this end-member. This value is in excellent agreement with its DFT-derived , but ~ 8% smaller than values as appearing in thermodynamic data bases. The DFT-computed superambient of Eas is given by the polynomial [in J/(mol K)] as follows: . A maximum excess enthalpy of mixing, Δ , of ~6 kJ/mol was derived for the Phl-Eas binary using line-broadening from IR spectra (wavenumber region 400-600 cm), which is in accordance with Δ determined from published solution-calorimetry data. The mixing behaviour can be described by a symmetric interaction parameter = 25.4 kJ/mol. Applying this value to published phase-equilibrium data that were undertaken to experimentally determine the Al-saturation level of biotite in the assemblage (Mg-Al)-biotite-sillimanite-sanidine-Qz, gives a = - 6358.5 ± 1.4 kJ/mol in good agreement with the independently DFT-derived value of = - 6360.5 kJ/mol. Application examples demonstrate the effect of the new activity model and thermodynamic standard state data, among others, on the stability of Mg-Al biotite + Qz.

摘要

通过将各种实验结果(量热法、红外光谱线宽展、现有相平衡数据分析)与密度泛函理论(DFT)计算相结合的综合方法,构建了一种新的镁铝黑云母活度模型。所得模型具有坚实的物理实验基础。它考虑了三个端元:金云母(Phl,KMg[(OH)AlSiO])、有序的伊斯特石(Eas,KMgAl[(OH)AlSiO])和无序的伊斯特石(dEas),因此包括了镁铝的有序-无序。由DFT得出的与Eas中M位上Mg和Al无序相关的无序焓Δ为34.5±3 kJ/mol。沿着Phl-Eas连线的各种黑云母成分在700℃和4千巴下进行了水热合成。合成的最富铝黑云母成分xAl = 0.77。样品通过X射线衍射(XRD)、微探针分析和红外光谱进行了表征。使用弛豫量热法在2至300 K的温度下测量了样品的热容(Cp),并在282至760 K之间进行了差示扫描量热法研究。根据对纯合成样品的低温测量确定,Phl在298.15 K时的量热(振动)熵为S = 319.4±2.2 J/(mol K)。Phl的标准熵S°为330.9±2.2 J/(mol K),这是通过添加由于四面体Al-Si无序产生的11.53 J/(mol K)的构型熵项得到的。该值比不同数据库中的值大1%,那些数据库依赖于对天然近Phl云母测量的较旧的量热数据。用这个新的S°重新分析Phl + 石英(Qz)稳定性的相平衡数据,得到Phl的标准生成焓ΔfH° = -6209.83±1.10 kJ/mol,比已发表的值负7 - 8 kJ/mol。Phl的超常温熵由多项式[S°/J/(mol K)]给出如下:......。在298.15 K时的量热熵沿Phl-Eas连线随成分线性变化,表明该二元体系中理想的振动混合熵。将这些结果线性外推到Eas成分,得到该端元的S = 294.5±3.0 J/(mol K)。该值与其DFT得出的值非常吻合,但比热力学数据库中出现的值小8%。Eas的DFT计算超常温熵由多项式[单位为J/(mol K)]给出如下:......。使用红外光谱(波数范围400 - 600 cm)的线宽展得出Phl-Eas二元体系的最大混合过剩焓ΔHm为~6 kJ/mol,这与从已发表的溶液量热法数据确定的ΔHm一致。混合行为可以用对称相互作用参数W = 25.4 kJ/mol来描述。将该值应用于已发表的相平衡数据,这些数据用于通过实验确定组合(Mg-Al)-黑云母-硅线石-透长石-Qz中黑云母的铝饱和水平,得到ΔfH° = -6358.5±1.4 kJ/mol,与独立的DFT得出的值ΔfH° = -6360.5 kJ/mol非常吻合。应用实例展示了新的活度模型和热力学标准态数据等对镁铝黑云母 + Qz稳定性的影响。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/7347/6707958/06d79c4fa49b/410_2019_1606_Fig1_HTML.jpg

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